Reduced mixing generates oscillations and chaos in the oceanic deep chlorophyll maximum

Green-belt development In many parts of the oceans a layer known as a ‘deep chlorophyll maximum’ develops about 50 to 100 metres below the surface as various opposing forces achieve a balance. Phytoplankton sinking from surface waters and taking nutrients with them meet an upward flux of nutrients f...

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Veröffentlicht in:	Nature 2006-01, Vol.439 (7074), p.322-325
Hauptverfasser:	Huisman, Jef, Pham Thi, Nga N., Karl, David M., Sommeijer, Ben
Format:	Artikel
Sprache:	eng
Schlagworte:	Animal and plant ecology Animal, plant and microbial ecology Biological and medical sciences Biomass Carbon - metabolism Chlorophyll Chlorophyll - metabolism Climate change Climate models Euphotic zone Fluctuations Fundamental and applied biological sciences. Psychology Global warming Hawaii Humanities and Social Sciences letter Marine multidisciplinary Nutrients Oceans Pacific Ocean Phytoplankton Phytoplankton - growth & development Phytoplankton - isolation & purification Phytoplankton - metabolism Plankton Population Dynamics Primary production Science Science (multidisciplinary) Sea water ecosystems Seasons Seawater - analysis Species composition Synecology Time Factors Water Movements
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